首页> 外文会议>Association of State Dam Safety Officials annual conference >DEVELOPMENT OF HYDROLOGIC HAZARD CURVES FOR ASSESSING HYDROLOGIC RISKS FOR STRATHCONA, LADORE FALLS AND JOHN HART DAMS ON THE CAMPBELL RIVER, BC
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DEVELOPMENT OF HYDROLOGIC HAZARD CURVES FOR ASSESSING HYDROLOGIC RISKS FOR STRATHCONA, LADORE FALLS AND JOHN HART DAMS ON THE CAMPBELL RIVER, BC

机译:用于评估Strathcona的水文风险的水文危险曲线,BC坎贝尔河上的妓女水文风险和约翰哈特水坝

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A stochastic flood model was developed for Strathcona, Ladore, and John Hart Dams on the Campbell River for use in developing flood-frequency estimates for extreme floods. The stochastic flood model utilized a deterministic flood computation model (UBC Watershed Model) and treated the hydrometeorological input parameters as variables instead of fixed values. Monte Carlo sampling procedures were used to allow the climatic and storm related input parameters to vary in accordance with that observed in nature. Hydrometeorological inputs that were treated as variables included: seasonality of storm occurrence; magnitude of extreme storm, temporal and spatial distribution of storms; temporal temperature pattern during the storm; sea-level and freezing level temperatures; hydrologic model antecedent conditions, and initial reservoir storage.The flood-frequency relationships generated by the flood model were used to estimate the Annual Exceedance Probability (AEP) of selected flood characteristics. The AEP for flood waters reaching the top of the lock blocks on Strathcona Dam (226.30 m) was estimated to be 1:5,500,000 and the annual probability of flood waters reaching the top of the impervious core (224.60 m) was estimated to be 1:34,000. The annual probability of overtopping at Ladore Dam (179.35 m) was estimated to be 1:960,000. The annual probability of overtopping of John Hart Dam (141.73m) was estimated to be 1:1,400,000 and overtopping of the impervious core, slurry wall and sheet piles (140.50m) was estimated to be 1:65,000.These flood magnitude-frequency curves are a valuable tool that bring the metric of a flood's probability, including the PMF, into the decision making process in regards to dam safety conditions. Given the speed at which computer model simulations can now be conducted, there are methods of analysis that can be efficiently implemented to refine the estimated AEP associated with extreme floods. The SEFM method is one such method that can provide dam owners with useful information to aid in dam safety decision making.
机译:在坎贝尔河上为Strathcona,Ladore和John Hart Dams开发了一种随机洪水模型,用于开发极端洪水的洪水频率估计。随机洪水模型利用了确定性的洪水计算模型(UBC流域模型),并将水流度输入参数视为变量而不是固定值。 Monte Carlo采样程序用于允许气候和风暴相关的输入参数根据本质上观察到的。被视为变量的水样投入包括:风暴发生的季节性;极端风暴,时间和风暴空间分布的幅度;风暴期间的时间温度模式;海平和冰冻水平温度;水文模型前进条件和初始储层储存。洪水模型产生的洪水频率关系用于估算所选洪水特征的年度超标概率(AEP)。估计到斯特拉希岛大坝(226.30米)锁定锁块顶部的AEP估计为1:5,500,000,估计洪水达到不透水核心(224.60米)的洪水的年度可能性估计为1: 34,000。在妓女大坝(179.35米)估计为1:960,000的年度概率。约翰哈特大坝(141.73米)估计的年约1,400,000件估计为1:1,400,000,估计为1:65,000.这些洪水级曲线(140.50m)估计为1:1,400,000是一个有价值的工具,可将洪水概率(包括PMF)的指标进入DAM安全条件的决策过程中。鉴于现在可以进行计算机模型仿真的速度,可以有效地实施分析方法以优化与极端洪水相关的估计AEP。 SEFM方法是一种这样的方法,可以提供具有有用信息的大坝所有者,以帮助大坝安全决策。

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